Meteorological history | |
---|---|
Formed | October 31,1997 |
Dissipated | November 9,1997 |
Severe tropical storm | |
10-minute sustained (JMA) | |
Highest winds | 95 km/h (60 mph) |
Lowest pressure | 985 hPa (mbar);29.09 inHg |
Cyclonic storm | |
3-minute sustained (IMD) | |
Highest winds | 65 km/h (40 mph) |
Category 1-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 120 km/h (75 mph) |
Overall effects | |
Fatalities | 3,275 total |
Damage | $385 million |
Areas affected | Philippines,Malaysia,Indonesia,Brunei,Vietnam,Cambodia,Thailand,Burma |
IBTrACS | |
Part of the 1997 Pacific typhoon and North Indian Ocean cyclone seasons |
Severe Tropical Storm Linda,also known as Typhoon Linda,Cyclonic Storm Linda (BOB 08),or in the Philippines as Tropical Depression Openg,was the worst typhoon in southern Vietnam in at least 100 years,killing thousands of people and leaving extensive damage. It formed on October 31,1997,in the South China Sea,between Indochina and the Philippines. Strengthening as it moved westward,Linda struck extreme southern Vietnam on November 2 with winds of 65 mph (105 km/h),dropping heavy rainfall. Once in the Gulf of Thailand it strengthened further to minimal typhoon status,but weakened to tropical storm strength before crossing the Malay Peninsula into the Bay of Bengal,the first storm to do so in five years. It restrengthened in the Indian Ocean to typhoon status,but increasing wind shear and weakened steering currents caused Linda to dissipate on November 9.
The worst of Linda's impact was in Vietnam,where 3,111 people were killed,and damage totaled 385 [1] [2] million (USD). Heavy rainfall caused flooding,which damaged or destroyed about 200,000 houses and left about 383,000 people homeless. Widespread crop and transportation damage also occurred,the latter which impeded relief efforts. Several countries around the world sent relief aid,including medical teams,food,and clothing. However,the food supply and health status of the storm victims proved not as bad as originally feared. Linda later struck Thailand,causing flash flooding and at least 164 deaths. The storm also affected Burma (Myanmar),Indonesia,Malaysia,and Cambodia to a lesser degree.
The origins of Typhoon Linda were from an area of convection that were first noted east of the Philippines on October 26. A subtropical ridge persisted to the north, which caused the disturbance to move generally westward. On October 29, the system crossed the Philippines and entered the South China Sea. It subsequently began to organize, and late on October 31, the Joint Typhoon Warning Center (JTWC) initiated advisories on Tropical Depression 30W. At that time, the system was located off the northwest coast of Borneo. [3] The PAGASA organization named it "Openg". [4]
Shortly after developing, the depression intensified into a tropical storm, and was named "Linda" by the JTWC. It continued to intensify, reaching winds of 65 mph (105 km/h) as it approached southern Vietnam. At 0900 UTC on November 2, Linda made landfall in the Vietnamese province of Cà Mau. It maintained its strength over land, and the storm quickly reached typhoon status after entering the Gulf of Thailand; a typhoon is a tropical cyclone with winds of at least 75 mph (121 km/h), although Linda did not intensify beyond minimal typhoon status. Turning northwestward, Linda deteriorated to tropical storm strength, and struck Thailand late on November 3 with winds of 65 mph (105 km/h). [3]
Linda weakened further over the mountainous terrain of the Malay Peninsula, and the storm emerged into the Andaman Sea with winds of 50 mph (80 km/h). This made Linda the first tropical cyclone since Tropical Storm Forrest in 1992 to cross from the western Pacific Ocean into the Indian Ocean. [3] Additionally, upon reaching the Indian Ocean, the India Meteorological Department (IMD) classified the storm as Cyclonic Storm BOB 08, with winds of 40 mph (64 km/h). [5] With warm waters, Tropical Storm Linda gradually re-intensified as it slowed down, due to a weakness in the subtropical ridge. On November 6, it again attained typhoon status while located off the southwest coast of Burma (Myanmar). [3] Initially, it was expected to cross the Bay of Bengal and make landfall near the India/Bangladesh border. [6] The cyclone only maintained peak strength for 18 hours, due to an increase in wind shear from a mid-latitude trough. Linda's motion became nearly stationary, and it gradually weakened for several days. On November 9, Linda dissipated about 375 miles (604 km) southwest of Yangon, Burma. [3] That day, the IMD also terminated advisories. [5]
Vietnam | 3,111 |
Thailand | 164 |
Total | 3,275 |
Prior to the arrival of the storm, officials in Vietnam issued warnings to the residents, although its approach was faster than expected, and the region rarely experiences tropical cyclones. Tropical Storm Linda dropped heavy rainfall across southern Vietnam, peaking at 9.17 inches (23.3 cm) in Cần Thơ. [7] The storm caused heavy damage in the country, particularly in the southernmost province of Cà Mau where it struck, [3] but also in Bạc Liêu, Sóc Trăng, and Kiên Giang. [8] The most severely affected regions were poor fishing communities. [9] Overall, the storm damaged 139,445 houses and wrecked 76,609 more, [10] which left 383,045 people homeless. [11] Thousands of schools were damaged, and 130,815 dykes were breached. [7] Additionally, the storm destroyed at least 3,122 boats. [10] The rainfall also flooded 1,750 square miles (4,500 km2) of rice paddy crop, about half of which in Cà Mau. [12] A preliminary damage total was estimated at 7.18 trillion dongs (US$385 million). [13]
Typhoon Linda caused considerable deaths in Vietnam. Many fishermen and sailors were caught at sea in the path of the storm, [3] unable to escape its path. [7] Within three days, the death toll in Vietnam was set at over 150, with thousands missing, [6] many of them fishermen. [12] By the fourth day after the storm, the toll reached 390, [8] and on November 14, eight days after the storm, the death toll reached 464. [10] Ultimately, the death toll was set at 3,111. [13] Eight days after Linda's passage, a United Nations Department of Humanitarian Affairs (DHA) report indicated 857 people were injured by the storm. [10] The government quickly established search and rescue teams, particularly for missing fishermen, and a total of 3,513 people were rescued after the storm. [7] In the weeks after the storm, hundreds of dead bodies washed ashore in Vietnam and Thailand. [14]
The Vietnamese government identified basic supplies that it needed in response to the storm; those included various foods, clothing, medicine, shelter supplies, and sanitation equipment. [8] The country made a formal request for international assistance, noting that the storm was the worst in 100 years, and officials had limited resources due to the unexpected destruction. [7] Prior to the request, the government of Switzerland sent about 500,000 Swiss francs (US$360,000) for immediate relief assistance. [12] Subsequently, ten other countries sent cash or relief supplies worth $2.6 million, including medical shelters from the United States, clothing from the United Kingdom, tents from Russia, and transport goods from Japan. [7] Red Cross workers had to travel by riverboat to bring aid to the most affected communities, [9] due to the poor state of the roads. [14] After two months, the Red Cross distributed 65,401 roofing sheets, 390 metric tons of rice, 11,990 mosquito nets, 6,871 blankets, 3,664 medical kits, and abundant clothing supplies to about 150,000 affected people; the supplies were purchased in Ho Chi Minh City. Eventually, the food supply and health status of the storm victims proved not as bad as originally feared. After the assistance was distributed, the Red Cross shifted focus toward reconstruction. Reconstruction was slow, partly due to a slowdown in economic activity from the Vietnamese New Year. Additionally, the two primary factories responsible for making iron and construction frames were only intermittently open, due to machines failing. [15] [16]
Elsewhere, moderate damage was also reported in Thailand, [3] where at least 12 casualties were reported on land, [14] and at least 152 fishermen were killed at sea. [17] Flash flooding occurred in six districts, which damaged about 88 square miles (230 km2) of croplands and destroyed 12 houses. Land transportation was affected, with 184 roads and 14 bridges damaged. The government of Thailand sent 20 medical teams to the most affected areas. [18] Following the storm, about 10,600 people became sick from flood related diseases. [19] Heavy rains fell in Tanintharyi Division in southeastern Burma (Myanmar), although because the winds were not strong, there was little damage. The typhoon increased smog and haze in Indonesia and Malaysia, which had been occurring for weeks. In Indonesia, the typhoon also removed atmospheric moisture, which lowered the chance for rain in areas affected by wildfires. [6] Cambodia was also affected by the outskirts of the storm. [12]
Extremely Severe Cyclonic Storm Mala was the strongest tropical cyclone of the 2006 North Indian Ocean cyclone season. In mid-April 2006, an area of disturbed weather formed over the southern Bay of Bengal and nearby Andaman Sea. Over a period of several days, the system became increasingly organized and was classified as a depression on April 24. Situated within a region of weak steering currents, the storm slowly intensified as it drifted in a general northward direction. It attained gale-force winds and was named Mala the next day. Conditions for strengthening improved markedly on April 27 and Mala subsequently underwent rapid intensification which culminated in the cyclone attaining its peak. Early on April 28, the cyclone had estimated winds of 185 km/h (115 mph). The Joint Typhoon Warning Center considered Mala to have been slightly stronger, classifying it as a Category 4-equivalent cyclone. Steady weakening ensued thereafter and the storm made landfall in Myanmar's Rakhine State on April 29. Rapid dissipation took place once onshore and Mala was last noted early the next morning.
Typhoon Chanchu, known in the Philippines as Typhoon Caloy, was the most intense typhoon in the South China Sea in the month of May according to the Hong Kong Observatory (HKO). The first named storm of the 2006 Pacific typhoon season, Chanchu formed on May 8 in the vicinity of the Federated States of Micronesia and progressed westward. It gradually intensified into a tropical storm and later severe tropical storm before moving through the Philippines. On May 13, Chanchu entered the South China Sea and became a typhoon, according to the Japan Meteorological Agency (JMA). Warm waters and favorable outflow allowed the storm to quickly intensify to peak maximum sustained winds of 175 km/h (109 mph) on May 15. Around that time, the typhoon turned sharply to the north toward southeastern China. Chanchu weakened as it curved to the northeast, making landfall near Shantou, Guangdong on May 17 as a severe tropical storm. The government of China considered Chanchu the earliest typhoon to make landfall in the province. On the next day, the storm emerged into the East China Sea, becoming extratropical on May 19 before dissipating west of Kyushu.
Typhoon Xangsane, known in the Philippines as Typhoon Milenyo, was a typhoon that affected the Philippines, Vietnam, and Thailand during the 2006 Pacific typhoon season. The name Xangsane was submitted by Laos and means elephant.
Typhoon Muifa, known in the Philippines as Typhoon Unding, was a strong typhoon during the 2004 Pacific typhoon season. The name Muifa is taken from the ume blossom.
Typhoon Durian, known in the Philippines as Super Typhoon Reming, was a deadly tropical cyclone that wreaked havoc in the Philippines and later crossed the Malay Peninsula in late November 2006, causing massive loss of life when mudflows from the Mayon Volcano buried many villages.
Typhoon Cecil, known in the Philippines as Tropical Storm Rubing, was one of two typhoons to strike Vietnam within a week in 1985. Cecil originated from an area of convection that tracked west-northwest and passed south of Palau late on October 9. The disturbance became increasingly defined as it moved through the southern Philippines. On October 12, a tropical depression developed, and the next day, the depression was upgraded into a tropical storm. Cecil turned northwest over the open waters of the South China Sea as it steadily strengthened, and was classified as a typhoon on October 14. After unexpectedly slowing down, Cecil continued to intensify and at noon of October 14, reached its peak intensity of 145 km/h (90 mph). Land interaction with Vietnam triggered a weakening trend. After turning west, Cecil moved onshore just north of Huế at 22:00 UTC on October 15. After tracking into Laos, the typhoon dissipated 39 hours later.
Severe Tropical Storm Cecil in May of 1989 caused devastating floods in central Vietnam, killing 751 people. The storm developed as a tropical depression over the South China Sea on May 22. Tracking north-northwestward, the system steadily intensified, attaining peak winds of 110 km/h (68 mph). The Joint Typhoon Warning Center (JTWC) assessed Cecil to have been slightly stronger with one-minute sustained winds of 140 km/h (87 mph). The storm made landfall near Hoi An, Vietnam early on May 25 and quickly weakened. The system later dissipated over Laos on May 26.
Typhoon Cimaron, known in the Philippines as Super Typhoon Paeng, was the most intense tropical cyclone to strike the Philippine island of Luzon since Typhoon Zeb in 1998. Originating from a tropical depression on October 25, Cimaron developed within an environment strongly favoring tropical cyclogenesis east of the Philippines. On October 28, the system underwent rapid intensification, culminating in attaining its peak strength with winds of 185 km/h (115 mph). Estimates from the Joint Typhoon Warning Center ranked the system as a Category 5-equivalent super typhoon with one-minute sustained winds of 260 km/h (160 mph), though this is argued to have underrepresented the typhoon's strength. The system moved ashore near Casiguran, Aurora in northern Luzon at peak strength. Crossing the island, Cimaron emerged over the South China Sea where conditions allowed for temporary reorganization. After becoming nearly stationary on November 1, the typhoon executed a tight anti-cyclonic loop and rapidly weakened. The storm degenerated into a tropical depression on November 4, before dissipating three days later off the coast of Vietnam.
Tropical Storm Podul, known in the Philippines as Tropical Depression Zoraida, was a weak but destructive tropical cyclone that affected the Philippines shortly after the devastating Typhoon Haiyan. The 31st named storm of the 2013 Pacific typhoon season, Podul developed as a tropical depression on November 11 between Palau and the Philippine island of Mindanao. The system moved west-northwestward and struck Davao Oriental in Mindanao on November 12, bringing heavy rainfall that killed two people and disrupted relief efforts following Haiyan. After crossing the Philippines, the depression intensified into Tropical Storm Podul on November 14. Shortly thereafter, the storm struck southeastern Vietnam, and its circulation dissipated on November 15. In Vietnam, Podul produced heavy rainfall that resulted in severe flooding. The storm damaged or destroyed 427,258 houses, and overall damage was estimated at 4.1 trillion₫. Podul killed 44 people in the country and caused 66 injuries.
The 2004 Myanmar cyclone was considered the worst to strike the country since 1968. The second tropical cyclone of the 2004 North Indian Ocean cyclone season, it formed as a depression on May 16 in the central Bay of Bengal. With low wind shear and a surge in the monsoon trough, the storm intensified while meandering over open waters. The storm eventually began a steady northeastward motion due to a ridge to the north over India. While approaching land, an eye developed in the center of the storm, indicative of a strong cyclone. On May 19, the cyclone made landfall along northwestern Myanmar near Sittwe, with maximum sustained winds estimated at 165 km/h (105 mph) by the India Meteorological Department. The storm rapidly weakened over land, although its remnants spread rainfall into northern Thailand and Yunnan province in China.
Extremely Severe Cyclonic Storm Forrest, also referred to as Tropical Storm Forrest while in the western Pacific basin before its Thai crossover, was a powerful tropical cyclone that prompted the evacuation of 600,000 people in Bangladesh in late November 1992. Originating from an area of disturbed weather near the Caroline Islands on November 9, Forrest was classified as a tropical depression three days later over the South China Sea. Tracking generally west, the system steadily organized into a tropical storm, passing Vietnam to the south, before striking Thailand along the Malay Peninsula on November 15. Once over the Bay of Bengal, Forrest turned northward on November 17 and significantly intensified. It reached its peak intensity on November 20 as a Category 4-equivalent cyclone on the Saffir–Simpson hurricane scale with winds of 230 km/h (140 mph). Hostile environmental conditions soon affected the cyclone as it turned abruptly east-northeastward. Forrest made landfall in northwestern Myanmar as a weakening system on November 21 before dissipating early the next day.
Severe Tropical Storm Talas was a tropical cyclone that affected Vietnam in mid-July 2017. The storm was first identified as a tropical disturbance over the South China Sea on July 13 and was upgraded to a tropical depression the following day. On July 15, the depression intensified into a named storm of the 2017 Pacific typhoon season. Before making landfall in Vietnam, Talas reached its peak intensity as a severe tropical storm on July 16. It weakened to an area of low pressure on July 17 as it moved inland. Throughout Vietnam, the storm resulted in 14 fatalities and damaged approximately 2,700 homes. Rough seas caused about 50 boats to sink. Nearly 50,000 hectares of vegetable fields, around 800 ha of aquaculture, and 47,600 ha of rice and other subsidiary crops were affected. The storm caused an estimated US$8.8 million in damages in Hainan province, China, increased rainfall in Myanmar and Thailand, and triggered landslides and flooding in parts of Central and Northern Laos.
Tropical Storm Sonca was a weak tropical cyclone that impacted Southeast Asia during the end of July 2017. As the 10th named storm of the 2017 Pacific typhoon season, Tropical Storm Sonca formed south of Hong Kong, after drifting westward for multiple days, the storm intensified into a tropical storm, receiving the name Sonca. The storm later affected Hainan, reaching its peak intensity. On July 25, the storm made landfall over the Quảng Trị province, then dissipated.
Typhoon Doksuri, known in the Philippines as Tropical Storm Maring, was a strong Category 2 typhoon that mostly impacted the Philippines and Vietnam during mid-September 2017. Forming as the nineteenth named storm of the season, Doksuri developed as a weak tropical depression over to the east of Visayas on September 10.
The 2020 Central Vietnam floods were a series of floods in Central Vietnam, which also affected some areas in Cambodia and Laos in October and early November 2020. The floods focused heavily in several provinces including Thừa Thiên Huế, Hà Tĩnh, Quảng Bình, Quảng Trị, and Quảng Ngãi. The floods were mainly caused by the seasonal monsoon, though enhanced by numerous tropical cyclones.
Severe Tropical Storm Usagi, known in the Philippines as Tropical Storm Samuel, was a tropical cyclone that affected the Philippines and Southern Vietnam in late November 2018, causing severe damage around the Visayas region and Ho Chi Minh City. The storm formed from a disturbance in the Central Pacific basin on November 3, but did not develop into a tropical storm until almost three weeks later, on November 13. Usagi underwent rapid intensification and peaked in intensity before making its final landfall on Vũng Tàu, Bà Rịa–Vũng Tàu province as a weakening tropical storm on November 25. While never considered as a typhoon by the Japan Meteorological Agency (JMA), the Joint Typhoon Warning Center (JTWC) assessed its intensity to be equivalent to Category 2 status on the Saffir–Simpson scale. Usagi caused one death and ₱52.2 million (US$992,000) in damages in the Philippines, most of which came from agriculture. Usagi caused 3 deaths and ₫925 billion in damages in Vietnam.
Tropical Storm Linfa was a weak, short-lived but deadly and destructive tropical cyclone that was the twelfth wettest tropical cyclone on record and the second of nine tropical cyclones in a row to strike Vietnam in 2020, a little under a month after the less damaging Tropical Storm Noul. The fifteenth named storm of the 2020 Pacific typhoon season, Linfa originated from a tropical depression which formed just to the west of the Philippines on October 6. After passing through the island nation, the storm emerged into the South China Sea and slowly gained strength, earning the name Linfa on October 10 on approach to Vietnam. On the next day, Linfa had reached peak strength and made landfall in Vietnam, marking the beginning of a devastating series of floods in the country and worsening the already active monsoon season. Linfa quickly dissipated as it moved inland, but associated thunderstorms continued for several days.
Tropical Storm Dianmu was a weak tropical cyclone that caused considerable damage over parts of Mainland Southeast Asia during late-September 2021. The fifteenth named storm of the 2021 Pacific typhoon season, Dianmu originated from an area of low-pressure situated in the South China Sea on September 21. Being first monitored by the Joint Typhoon Warning Center, the system rapidly consolidated to a tropical depression on September 22 as it continued to approach Vietnam before strengthening further to a weak tropical storm, with the Japan Meteorological Agency naming it as "Dianmu". Little intensification occurred before it made landfall on the country with winds of 35 knots. It then rapidly weakened over land and dissipated on September 24 as a tropical cyclone.
Vietnam is a southeast Asian country, and is the easternmost country of mainland Southeast Asia. It borders the South China Sea, hence, seeing the increased likeliness of tropical cyclones. Tropical cyclones in this area are considered to be part of the Northwest Pacific basin, and therefore, storms here are considered as typhoons.
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